FN Archimer Export Format
PT J
TI Modelled and observed sea surface fCO2 in the southern ocean: a comparative study
BT 
AF LOUANCHI, F
   HOPPEMA, M
   BAKKER, DCE
   POISSON, A
   STOLL, MHC
   DE BAAR, HJW
   SCHAUER, B
   RUIZ-PINO, DP
   WOLF-GLADROW, D
AS 1:1;2:2;3:3;4:1;5:4;6:4;7:1;8:1;9:5;
FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;
C1 UPMC CNRS, URA 2076, Phys & Chim Marines Lab, F-75252 Paris 05, France.
   Univ Bremen, FB1, IUP, Dept Tracer Oceanog, D-28334 Bremen, Germany.
   CNRS ORSTOM UPMC, Lab Oceanog Dynam & Climatol, F-75252 Paris 05, France.
   Netherlands Inst Sea Res, NL-1790 AB Den Burg, Netherlands.
   Alfred Wegener Inst Polar & Marine Res, D-27570 Bremerhaven, Germany.
C2 UNIV PARIS 06, FRANCE
   UNIV BREMEN, GERMANY
   CNRS, FRANCE
   INST SEA RESEARCH (NIOZ), NETHERLANDS
   INST A WEGENER, GERMANY
IF 3.256
TC 22
UR https://archimer.ifremer.fr/doc/00273/38452/36836.pdf
LA English
DT Article
CR CIVA 1 - MD 74
   INDIGO 3 - MD 53
BO Marion Dufresne
AB The results of an existing one-dimensional diagnostic model that calculates the fugacity of CO2 (fCO2) in the surface layer of the southern ocean were compared with in situ observations from different ocean sectors and seasons. Our model is based on the translation of monthly variations of constraints fields into surface water fCO2 variations, and was used to assess the CO2 uptake of the southern ocean. In situ observations are useful to verify the model results and were here applied to improve the estimation of the CO2 uptake of the southern ocean south of 50°S. The model reproduces the fCO2 distribution in both Pacific and Indian sectors of the southern ocean satisfactorily, the mean deviation being only 5 matm. This discrepancy requires only a minor modification of the CO2 uptake calculated by the model for that area. By contrast, the model strongly underestimates the fCO2 levels in early spring and early winter in the Weddell gyre. This indicates that the CO2 uptake by the Atlantic sector of the southern ocean as calculated by the model, amounting to 0.47 GtC yr−1, should be reduced, possibly by about half of this value. The reason for this mismatch lies in the use of climatological physical constraints by the model, that do not sufficiently well describe reality. Partly, the mismatch is also caused by a difference of seasonal stage between the model which reflects climatological conditions and the real ocean which is affected by interannual variability. Based on this study it is concluded that the CO2 uptake of the southern ocean south of 50°S is likely to lie somewhere between 0.6 and 0.7 GtC yr−1 for the 1990s, which is a high value compared to estimates from other investigations.
PY 1999
PD APR
SO Tellus Series B-chemical And Physical Meteorology
SN 0280-6509
PU Munksgaard Int Publ Ltd
VL 51
IS 2
UT 000081143400029
BP 541
EP 559
DI 10.1034/j.1600-0889.1999.00029.x
ID 38452
ER

EF